溶蚀的 meaning in Chinese
corroded
Examples
- Besides lithological characters and geological structures , the karst development and groundwater in the area are affected by neotectonic movement and fossil karst
区内岩溶发育和地下水赋存除受岩性、地质构造的控制外，还受新构造运动和古溶蚀的影响。 - Test of carbonate rock sample ' s dissolution reveals that lithology ' s effects on dissolution mainly lie on their different start - up dissolution velocities
摘要对碳酸盐岩类岩石样品的溶蚀试验表明，岩性对溶蚀的影响主要表现为各类岩石在启动溶蚀速率上的差异。 - The process of diagenesis controlled partly by sedimentation , the evolution of pores influenced by it . the affection of origin ingredient and structure in sand to sediment and solution in gooey be exhibited
长6储层砂体中沉积作用对于成岩进程的控制，主要表现在砂岩的原始成分和结构对于胶结物的沉淀和溶蚀的影响。 - For the high pressure phase equilibrium system composed of co2 , h2o , cacl2 , etc . , co2 is treated as super critical fluid truly , the volume of which is estimated by bwr state equation suitable for super critical fluid
考虑了酸液溶蚀的碳酸盐以及酸岩反应生成的二氧化碳对人工裂缝体积的影响，针对裂缝内由二氧化碳、水、氯化钙等物质组成的高压相平衡体系，将二氧化碳真实地处理为超临界状态，其体积由适用于超临界流体的bwr状态方程求解。 - Then , by the comprehensive analysis of essential conditions for stone forest development , and the quantitative study on the evolution phases of bajiang karst catchment and the spacial coupling analysis of its hydro - geomorphological system , the paper studies the relationship between the evolution of bajiang karst drainage area and the development of stone forest , and , combined with the evolution history of the catchment , puts forward a model concerning the relationship between the evolution of bajiang karst catchment and stone forest development , in the mechanism of " tri - level erosion " , if a < s < c , the visible and actual height of stone pillars will keep on increasing , meanwhile , soil layer among stone pillars will become thicker and thicker , so the the height of stone pillars " root will become higher and higher , too
在“三重剥蚀”机制中，若a s c ，石柱的可见高度和实际高度会不断增高，同时，石柱的根部的土层会增厚，其土下部分的高度也会不断增大。若a c s ，说明石柱的实际高度在增加的同时，其可见高度也在增加，但土层会变得越来越薄，最终当底土被完全剥蚀掉后，气下溶蚀和土下溶蚀的差异消失，此时a接近于c ，石柱的实际高度将停止拔高或极缓慢增长，并在各种物理、化学风化的作用下而变得日益矮小。若s a c ，石柱的可见高度将趋于变矮，但驱动石林发育的土层厚度将会增大。